Rock Identifier
Likely labradorite-bearing rock (Labradorite (plagioclase feldspar; approximately (Ca,Na)(Al,Si)₄O₈)) — igneous
igneous

Likely labradorite-bearing rock

Labradorite (plagioclase feldspar; approximately (Ca,Na)(Al,Si)₄O₈)

AI-generated identification · may be incorrect

Dark gray to black, rough specimen with silvery-blue flashes consistent with feldspar iridescence (labradorescence). Labradorite has Mohs hardness 6–6.5, vitreous-to-pearly luster, triclinic crystals, and two cleavage directions; the image alone cannot confirm the identification or whole-rock composition.

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Physical properties

Dark gray to black, rough specimen with silvery-blue flashes consistent with feldspar iridescence (labradorescence). Labradorite has Mohs hardness 6–6.5, vitreous-to-pearly luster, triclinic crystals, and two cleavage directions; the image alone cannot confirm the identification or whole-rock composition.

Formation & geological history

Labradorite crystallizes from cooling magma, commonly in anorthosite and related igneous rocks; these rocks formed in many geological settings and ages.

Uses & applications

Labradorite is used as a decorative and ornamental stone, in jewelry and carvings, and as a collectible mineral.

Geological facts

Its blue-green flashes arise from light interference within microscopic feldspar layers, not from a surface coating.

Field identification & locations

Look for broad blue or silver flashes that change with viewing angle, plus feldspar cleavage; notable sources include Labrador, Canada, and Madagascar. This small, unpolished piece appears suitable for a modest specimen collection.